Tropical cirrus and water vapor: an effective Earth infrared iris feedback?
We revisit a model of feedback processes proposed by Lindzen et al. (2001), in which an assumed 22% reduction in the area of tropical high clouds per degree increase in sea surface temperature produces negative feedbacks associated with upper tropospheric water vapor and cloud radiative effects....
Main Authors: | Q. Fu, M. Baker, D. L. Hartmann |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2002-01-01
|
Series: | Atmospheric Chemistry and Physics |
Online Access: | http://www.atmos-chem-phys.net/2/31/2002/acp-2-31-2002.pdf |
Similar Items
-
Reply to: 'Tropical cirrus and water vapor: an effective Earth infrared iris feedback?'
by: M.-D. Chou, et al.
Published: (2002-01-01) -
Tropical thin cirrus and relative humidity observed by the Atmospheric Infrared Sounder
by: K. N. Liou, et al.
Published: (2008-03-01) -
Cirrus and water vapor transport in the tropical tropopause layer – Part 1: A specific case modeling study
by: T. Dinh, et al.
Published: (2012-10-01) -
The impact of cirrus clouds on tropical troposphere-to-stratosphere transport
by: T. Corti, et al.
Published: (2006-01-01) -
On the importance of small ice crystals in tropical anvil cirrus
by: E. J. Jensen, et al.
Published: (2009-08-01)